APPENDIX. 



279 



as 

 lis 

 lit 

 Id 



2. Erian Flora. 



(1) Upper Erian Suh-Flora : 



This corresponds to the Catskill and Chemung of the New York 

 series, and to the Upper Devonian of Europe. 



The flora of this formation, which consists mostly of sandstones, 

 is not rich. Its most distinctive species on both sides of the Atlantic 

 seem to be the ferns of the genus Archcpopteris, along with species 

 referred to the genus Cyclopteris, but which, in so far as their barren 

 fronds arc concerned, for the most part resemble Archceopferis. 



The characteristic American species are Archceopteris Jacksoni, 

 A. Rogersi, and A. Gaspiensis. VycJopteris obtusa and C. (Platy- 

 phyllum) Brou lii are also very characteristic species. In Europe, 

 Archceopteris Hibernica is a prevalent species. 



Leptophleum rhombicum and fragments of Psilophyton are also 

 found in the Upper Erian. There is evidence of the existence of 

 vast numbers of Rhizocarps in this period, in the deposits of spore- 

 cases (Sporangites Iluronensis) in the shales of Kettle Point, Lake 

 Huron ; and in deposits of similar character in Ohio and elsewhere 

 in the West. 



The Upper Erian flora is thus very distinct from that of the 

 Lower Carboniferous, and the unconformable relation of the beds in 

 the Northeast may perhaps indicate a considerable lapse of time. 

 Still, even in localities where there appeal's to be a transition from 

 the Carboniferous into the Devonian, as in the Western States and 

 in Ireland, the characteristic flora of each formation may be distin- 

 guished, though, as already stated, there is apparently some mixture 

 in the South. 



(2) Middle Erian Sub-Flora : 



Both in Canada and the United States that part of the great 

 Erian system wiiich may be regarded as its middle division, the 

 Hamilton and Marcellus shales of New York, the Cordaites shales of 

 St. John, New Brunswick, and the middle shales and sandstones of 

 the Gaspe series, presents conditions more favourable to the abundant 

 growth of land-plants than either the upper or lower member. In 

 the St. John beds, in particular, there is a rich fern flora, comparable 

 with that of the coal-formation, and numerous stipe3 of ferns and 

 trunks of tree-ferns have been found in the Hamilton and Cornifer- 

 ous series in the West, as well as trunks of Dadorylon, It is, how- 

 ever, distinguished by a prevalence of small and delicate species, and 

 by such forms as HymenophyUites and the smaller Sphenopterids» 

 and also by some peculiar ferns, as Archo'opteris and Megalopteria. 



